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22
Matti Sauramo, The mode of the land upheaval in Fennoscandia.
the earth’s ernst, the diminishing ice-sheet having chiefly controlled
the rate and mode of the land uplift. The isostatic recovery has,
however, not progressed like a wave after the retreating ice margin;
it is discontinuous in another manner. There are two limited areas
Fig. 9. Map showing some of the most important structures in the deformation
of the earth’s crust during late-glacial time. The toothed line indicates the ice
margin at the close of the first Salpausselkä stage.
which have been tilted separately one after the other during a
relatively short time; hence the uplift of the earth’s crust took place at
a slower rate throughout the uncovered area. Moreover, the
hinge-lines run in the first place parallel with the isobases, but at the same
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